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Rheological Properties of the Silica phases in Clinker slurries. Helge Hodne

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ANNUAL TRANSACTIONS OF THE NORDIC RHEOLOGY SOCIETY, VOL. 11, 2003

Rheological Properties of the Silica phases in Clinker slurries.

Helge Hodne1and Arild Saasen2

1-Stavanger University College, Pb.8002, NO-4068 Stavanger, Norway 2-Statoil, NO-4035 Stavanger Norway

ABSTRACT

The setting time of cement slurries is controlled by the addition of gypsum to the clinker during the grinding process. This addition has a different influence on the various constituents of the clinker. We have studied the rheological properties of triclinic and monoclinic C3S, the main constituents of the clinker phase, and compared their behaviour with that of a Class G clinker.

INTRODUCTION

The first stage in the manufacture of cement is the production of the clinker. The raw materials consist of various rock minerals rich in calcium and silica. The minerals are fed into a roller oven where they are heated to approximately 1500 ºC, at such a high temperature the minerals are partly melted. Thereafter follows a section where the minerals are cooled at a controlled rapid rate. Because of rapid cooling these minerals are unstable and re- crystallize when water is added. The product that comes out of the oven is called clinker and it consists of a balanced mixture of amorphous and crystalline compounds. The particle size of the clinker varies from powder to pebbles of centimetre size.

The production of cement from the clinker comprises the grinding of clinker together with minerals mainly containing gypsum.

The gypsum in cement affects the setting time, the strength development and the volume stability1.

Alite or C3S as written in the abbreviated form used in cement chemistry is the most important constituent of all normal Portland cement clinkers, of which it constitutes 50- 70%. It is Ca3SiO5 or tricalcium silicate. In pure compounds, when cooled to room temperature only the triclinic structure is present. In production clinkers, due to the incorporation of foreign ions, the form present at room temperature is normally the monoclinic structure. However, the triclinic structure is also present. Thus, the pure monoclinic C3S we used was Al2O3+MgO stabilized. In this study we also used a Portland cement for comparison. This was an API-specified2 Class G cement.

EXPERIMENTAL CONDITIONS Sample preparation

The clinker, the gypsum and the anhydrite used were all delivered by Norcem AS. They are used as the basic constituents in the production of Class G cement, as specified by API2. Before measurement they were all ground separately by the use of a Tecon, 400VL ball mill. The particle size used in our experiments, if otherwise not stated, were the fraction that during dry sieving passed through a sieve with a mesh of 75 micron.

The Class G cement used was also delivered by Norcem AS. The Class G cement has a Blaine surface area of 320 m2/kg. Before measurement it was also dry sieved through a mesh of 75 micron.

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The monoclinic and triclinic C3S used were laboratory minerals delivered by Construction Technology Laboratories, Inc.

in Skokie, Illinois. The samples were delivered as pure compounds having a measured specific Blaine surface area of 299 and 313 m2/kg for the monoclinic and the triclinic C3S respectively. The monoclinic C3S had been stabilized by Al2O3 and MgO.

Before use the samples were dry sieved through a mesh of 45 micron.

For the rheological testing, samples of 10 ml were made. They were first vigorously stirred by hand in the measuring cup for 30 seconds giving a homogenous test sample. Only the monoclinic C3S had to be hand stirred for 60 seconds before it resulted in a homogenous test sample. After hand mixing the samples were placed in the rheometer and sheared for 60 seconds at a shear rate of 1020 s-1. The samples were then measured at a constant shear rate of 51 s-1.

The solid phase volume fraction of all the samples was 0.419. The specific density used was 3.12 kg/m3 for the triclinic C3S and 3.15 kg/m3 for all the other cement materials.

For all samples distilled water was used and all experiments were carried out at a temperature of 25˚C.

Viscosity measurements

The rheological properties of the slurries were measured using a Physica UDS 200 rheometer (Physica Meȕtechnik GmbH, Stuttgart) fitted with a concentric cylinder configuration named Z3 DIN. All tests were done within ±0.5°C of the set temperature.

Zeta potential measurements

The zeta potential was measured by use of an AcoustoSizer from Colloidal Dynamics, Warwick, RI, USA. All tests were done within ±1.0°C of the set temperature. The samples were mixed in accordance with API2.

RESULTS

Viscosity measurements

In Fig. 1 the viscosity development of the clinker as a function of time is plotted at a constant shear rate of 51s-1. The measurements start approximately 200 seconds after the clinker and water was initially mixed. Three different samples of the same composition were measured at various durations of time. All three series indicate the same time dependant development of the viscosity.

0 0,5 1 1,5 2 2,5 3 3,5

0 500 1000 1500 2000 2500

Time [s]

Viscosity [Pas] Sample 1

Sample 2 Sample 3

Figure 1. Viscosity development as a function of time for a Class G clinker measured at a constant shear rate of 51 s-1.

During the first approximately 300 seconds of measurement there is a marked increase in the viscosity followed by a decrease and a stabilisation at a slightly higher value than the initial. In this period the viscosity increases from an initial value slightly below 0.5 Pas to a maximum in the range of 2.7 to 3.1 Pas followed by a decrease and apparent stabilisation around 0.8 to 1.3 Pas.

In Fig. 2 the effect of adding gypsum and anhydrite to the clinker is shown. The clinker has been added 4 and 3.2% by weight of gypsum and anhydrite respectively the latter being reduced thus adding a comparable amount of calcium to the clinker. Also a sample of Class G cement from Norcem AS was measured for comparison. The Class G cement consists of clinker that has been added gypsum. All

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three curves represent the average values of two different measurements.

0 0,2 0,4 0,6 0,8 1 1,2

0 200 400 600 800 1000 1200 1400 Time [s]

Viscosity [Pas]

Clinker + Gy ps um Clas s G Cement Clinker + A nh ydrite

Figure 2. Viscosity development at a shear rate of 51 s-1as a function of time for a

Class G clinker added gypsum and anhydrite, and for a Class G cement.

The effect of adding gypsum and anhydrite to the clinker is profound as can be seen when comparing the measured values in Fig. 2 with those in Fig.1 The initial measured viscosity at 200 seconds and the measured viscosity after 1360 seconds are within the same range, but the rapid increase to a maximum value followed by a decrease can no longer be found.

When comparing the effect of adding gypsum to the clinker with that of adding anhydrite we see that adding gypsum gives initially a larger reduction in the viscosity but the difference is somewhat reduced towards the end of the measuring period.

When comparing the effect of adding gypsum and anhydrite to clinker with the measured values of the Class G cement we see that the Class G cement viscosity is the lowest.

In Fig. 3 the viscosity development of both the triclinic and the monoclinic C3S phases as a function of time has been measured. All four curves represent the average values of two different measurements. Both the monoclinic and the triclinic C3S show an increase in viscosity during the measured interval, monoclinic C3S showing the highest viscosity. The effect of adding

gypsum is also shown. For the monoclinic C3S the adding of gypsum results in a marked drop in viscosity while for triclinic C3S the adding of gypsum results in lower viscosity in the beginning of the measuring period and a higher viscosity towards the end of the period.

0 0,5 1 1,5 2 2,5

0 200 400 600 800 1000 1200 1400

Time [s]

Viscosity [Pas]

Monoclinic C3S Monoclinic C3S + Gypsum Triclinic C3S Triclinic C3S + Gypsum

Figure 3. Viscosity development at a shear rate of 51 s-1as a function of time for a monoclinic and a triclinic C3S, with and

without gypsum added.

When comparing the measured viscosity of the silica phases in Fig. 3 with that of the clinker shown in Fig. 1 we see that neither the triclinic nor the monoclinic C3S show the same marked increase followed by a decrease of the viscosity as that of the clinker during the measured interval.

The zeta potential of a 1% by volume clinker slurry was also measured. This clinker was dry sieved through a sieve with a mesh of 20 micron before measurement and only one sample was measured. The time period of measurement was from approximately 225 seconds after initial mixing till 4100 seconds. Only one sample was measured. The zeta potentials were measured subsequently 19 times during this period and were measured to approximately +4 mV. During this period they showed no marked development as a function of time.

DISCUSSION

The behaviour of the Class G clinker as illustrated in Fig. 1, with the rapid increase

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followed by a decrease in the viscosity is expected to be due to a flocculation of the clinker particles followed by a partial de flocculation. This is in accordance with Yang et al4 who found that normal neat cement suspensions are either flocculated or coagulated and that the degree of flocculation or coagulation is not sensitive to the variation of the zeta potential, for zeta potentials between –20 mV and +20 mV.

Our measurement of the zeta potential lying well within this range further confirms this assumption.

The adding of gypsum and anhydrite to the clinker, as shown in Fig. 2 is thus, expected to hinder the rapid onset of a reversible flocculation.

The lower initial viscosity of the gypsum added clinker slurry in Fig. 2 compared with the anhydrite added slurry is expected to be due to the more rapid dissolution of gypsum in water at this temperature. Saasen et al3 observed the same tendency at 22ºC but at a temperature of 52ºC they observed a different behaviour. This behaviour is not thoroughly understood.

The Class G slurry in Fig. 2 developed viscosity following a similar trend.

However, the viscosity is lower; possibly due to a different particle size distribution.

The triclinic C3S is the stable end product of the calcium silicate phase from the oven. It has a perfect C3S composition and should not react with gypsum. With the same solid fraction we see no significant difference in viscosity fore the pure triclinic C3S curve with and without added gypsum.

The reduction in reaction of the monoclinic C3S in Fig.3 on the addition of gypsum is more profound. This C3S phase is stabilized using impurities and is thus more similar to clinker than triclinic C3S is. However, we have no evidence whether the gypsum phase reacts with the impurities or the structure itself.

CONCLUSION

We have shown that the rheological behaviour to the clinker phase depends on the sulphate source. This was found not to be due to sulphate reaction with the triclinic C3S

We have found an initial flocculation of the clinker phase that is diminished by the addition of a sulphate source.

REFERENCES

1. Taylor, H.F.W., (1990) "Cement Chemistry", Academic Press Ltd., London, p. 234.

2. American Petroleum Institute, (1990), Specifications for Materials and Testing for Well Cements, API Spec. 10, Fifth ed., Washington DC, July 1.

3. Saasen, A, Haugom, J.O. and Johansen, E. (1994), “The Effect of Gypsum and Anhydrite on Rheological Properties of Cement Slurries”, Ann. Trans. Nordic Rheology Society, 2, 85-87.

4. Yang, M., Neubauer, C.M. and Jennings, H.M., (1997), “Interparticle Potential and Sedimentation Behavior of Cement Suspensions”, Elsevier, Advn. Chem. Bas.

Mat.,5, 1-7 .

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